Solar Interior

The solar interior cannot be observed directly. Our knowledge is based on mathematical models. The solar interior can be separated into three large zones. Energy is generated in the core (1) by nuclear reactions. The conversion of hydrogen to helium is the dominant nuclear reaction (97% of radiated solar energy). About half billion tuns of hydrogen is changed to helium every second. Nuclear reactions are highly sensitive to temperature and density. Two individual hydrogen nuclei must collide with enough energy to overcome the repulsive electrical force between positively charged nuclei and to form helium nucleus. The temperature at the very center of the Sun is about 15,600,000 K and the density is approximately 150 g/cm3. The temperature drops to half its central value at distance 175,000 km from the center (about 25% of the distance from center to the photosphere) and the density drops to about 1/8 of its central value. Nuclear reactions practically shut off and therefore the edge of the solar core is defined at this distance. The energy generated in the solar core is at first transported by means of radiation. The so called radiative zone (2) extends up to 70% of the distance from the solar center to the photosphere. The energy is carried by photons (mostly gamma-rays and x-rays) which bounce from particle to particle through the radiative zone. Although the photons travel at the speed of light they bounce so many times that an individual photon takes about a million years to come through the radiative zone. The temperature of radiative zone bottom is about 7,000,000 K, at the top "only" 2,000,000 K. The density drops down from 20 g/cm3 to only 0.2 g/cm3. The opacity of the solar material increases with distance from the solar center and at the top of radiative zone the opacity is so hight that the transport of energy by radiation is ineffective. The high opacity is a consequent of relatively "low temperature". Heavier atoms are not totally ionized and they are able to hold some of their electrons which makes the material more opaque. Convection is the method of energy transport in this opaque material (ascending and descending flows - "boiling motion"). The convection zone (3) is the outer-most layer of solar interior. It extends from a depth of about 200,000 km up to the visible surface. The temperature drops in this layer from 2,000,000 K down to 5,700 K and the density from 0.2 g/cm3 drops down to 0.0000002 g/cm3. The radiative and convective zone are separated by so-called interface layer. It is now believed that the solar magnetic field is generated in this layer.